Winter warming in Alaska accelerates lignin decomposition contributed by Proteobacteria

  • Mengting M. Yuan (Contributor)
  • Yiqi Luo (Contributor)
  • Colin T. Bates (Contributor)
  • Eric R. Johnston (Contributor)
  • Linwei Wu (Contributor)
  • Daliang Ning (Contributor)
  • Jiajie Feng (Contributor)
  • Rosvel Bracho (Contributor)
  • Fenliang Fan (Contributor)
  • Yunfeng Yang (Contributor)
  • Lauren Hale (Contributor)
  • Jiesi Lei (Contributor)
  • James M. Tiedje (Contributor)
  • Gangsheng Wang (Contributor)
  • Qun Gao (Contributor)
  • Christopher Penton (Contributor)
  • Jizhong Zhou (Contributor)
  • Renmao Tian (Contributor)
  • Xuanyu Tao (Contributor)
  • Julian Yu (Contributor)
  • Konstantinos T. Konstantinidis (Contributor)
  • E. A G Schuur (Contributor)
  • James R. Cole (Contributor)

Dataset

Description

Abstract Background In a warmer world, microbial decomposition of previously frozen organic carbon (C) is one of the most likely positive climate feedbacks of permafrost regions to the atmosphere. However, mechanistic understanding of microbial mediation on chemically recalcitrant C instability is limited; thus, it is crucial to identify and evaluate active decomposers of chemically recalcitrant C, which is essential for predicting C-cycle feedbacks and their relative strength of influence on climate change. Using stable isotope probing of the active layer of Arctic tundra soils after depleting soil labile C through a 975-day laboratory incubation, the identity of microbial decomposers of lignin and, their responses to warming were revealed. Results The β-Proteobacteria genus Burkholderia accounted for 95.1% of total abundance of potential lignin decomposers. Consistently, Burkholderia isolated from our tundra soils could grow with lignin as the sole C source. A 2.2 °C increase of warming considerably increased total abundance and functional capacities of all potential lignin decomposers. In addition to Burkholderia, α-Proteobacteria capable of lignin decomposition (e.g. Bradyrhizobium and Methylobacterium genera) were stimulated by warming by 82-fold. Those community changes collectively doubled the priming effect, i.e., decomposition of existing C after fresh C input to soil. Consequently, warming aggravates soil C instability, as verified by microbially enabled climate-C modeling. Conclusions Our findings are alarming, which demonstrate that accelerated C decomposition under warming conditions will make tundra soils a larger biospheric C source than anticipated. Video Abstract
Date made availableJun 5 2020
Publisherfigshare Academic Research System

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